About fifteen miles Southeast of the town
of Salem in Southeastern Missouri, near the junction of Dent County
Roads 559 & 560, a spring-fed brook begins its journey North. Before
long, the brook merges with the ‘Dry Branch’ (on the right), ‘Wofford
Branch’ and ‘Carty Branch’ (both on the left) and becomes the source
of the Meramec River. For many millions of years the Meramec has been
carving its twisting, sometimes tortuous 240 mile course into the solid
rock of the Ozark Plateau, scouring its way through a deep, slowly widening
valley, bordered by limestone bluffs and steep hills. It is joined along
the way by innumerable springs, creeks, and four large tributaries,
which transform the Meramec into a one hundred yard - to two hundred
yard wide flood plane stream at its confluence with the Mighty Mississippi
eighteen miles below St. Louis.
Maramec spring (note the spelling) is the
first of the four major contributors, it pours an average volume of
one hundred million gallons of cold clear water into the Meramec per
day, swelling the river to twice its size. It is interesting to note
that the Dry Fork, which is about the same size as the Meramec in that
area, loses most of its volume underground to become a major contributor
to Maramec Spring, and in a round-about way - a major contributor to
the Upper Meramec. Over the next thirty miles, the inflows from many
smaller branches turn the river into a prime stream. Then, from the
right, the translucent waters of the second and largest of the headwater
contributors, the Courtois--(pronounced code-away)--Huzzah creek, mingles
with the Meramec, giving it the impression of a truly big river. Swirling
on past Onondaga Cave (Leasburg), Meramec State Park (Sullivan), and
the Meramec Caverns (Stanton)--all on the left-- the Meramec receives
the cloudy waters of the Bourbeuse River--its only major contributor
from the west. As the darker waters flow on, the valley widens, and
the river becomes a series of long, slow, wide pools, connected by short,
fast, riffles. Around twenty-five miles below the Bourbeuse River confluence,
the last major contributor, the Big River, flows into the Meramec from
the right. Now, even wider and more sluggish, it enters the Mississippi
flood-plain, and wends its way another thirty miles before draining
into the Mississippi.